198919931967199619641961197819951958197119861959198719971965200219661980199119732005198519791974197019821994198319601977196820031975200419921999200119842000198819631969196219901972197619981981northward-movement-of-marine-speciesFalse2008-07-21T09:24:56ZFalse2008 2.3.1Falseclimatenorthward-movement-of-marine-species Northward movement of marine species (CLIM 015) - Assessment published Sep 2008 Increases in regional sea temperatures have triggered a major northward movement of warmer-water plankton in the north-east Atlantic and a similar retreat of colder-water plankton to the north. This northerly movement is about 10 o latitude (1 100 km) over the past 40 years, and it seems to have accelerated since 2000. This will have an impact on the distribution of fish in the region. Many species of fish and plankton have shifted their distributions northward. Sub-tropical species are occurring with increasing frequency in European waters and sub-Arctic species are receding northwards. The rate of northward movement of a particular species, the silvery john dory, has been estimated at about 50 km/year. Changes in the geographic distribution of some species of fish have been observed and may affect the management of fisheries. Fisheries regulations in the EU include allocations of quotas based on historic catch patterns, and these may need to be revised. climate change north sea plankton marine fisheries CLIM CLIM015 015 2008-09-07T22:00:00Z4OFS.interfaces.IFindSupportApp.interfaces.IUndoSupportpersistent.interfaces.IPersistentOFS.interfaces.ICopyContainerProducts.Archetypes.interfaces.base.IBaseFolderProducts.CMFPlone.interfaces.constrains.ISelectableConstrainTypesProducts.CMFCore.interfaces._content.IMutableMinimalDublinCoreplone.contentrules.engine.interfaces.IRuleAssignableProducts.LinguaPlone.interfaces.ITranslatableProducts.CMFCore.interfaces._content.IContentishApp.interfaces.INavigationProducts.NavigationManager.sections.interfaces.INavigationSectionPositionableeea.cache.subtypes.interfaces.ICacheAwareOFS.interfaces.IObjectManagereea.themecentre.interfaces.IPossibleThemeCentreProducts.CMFCore.interfaces._content.ICatalogAwareplone.locking.interfaces.ITTWLockablearchetypes.schemaextender.interfaces.IExtensibleeea.faceted.inheritance.subtypes.interfaces.IPossibleFacetedHeritorProducts.CMFCore.interfaces._content.IWorkflowAwareProducts.ATContentTypes.interfaces.interfaces.IATContentTypeeea.alchemy.interfaces.IAlchemyDiscoverablewebdav.interfaces.IWriteLockplone.folder.interfaces.IOrderableFolderProducts.CMFCore.interfaces._content.IOpaqueItemManagereea.promotion.interfaces.IPromotableeea.reports.interfaces.IPossibleReportContainerplone.app.iterate.interfaces.IIterateAwareeea.versions.interfaces.IVersionEnhancedApp.interfaces.IPersistentExtraProducts.CMFCore.interfaces._content.IDynamicTypeeea.uberlisting.browser.app.interfaces.IPossibleUberlistingViewProducts.CMFDynamicViewFTI.interfaces.ISelectableBrowserDefaulteea.annotator.subtypes.interfaces.IAnnotatorAwareplone.app.folder.folder.IATUnifiedFolderAccessControl.interfaces.IOwnedzope.annotation.interfaces.IAttributeAnnotatableAcquisition.interfaces.IAcquirereea.relations.content.interfaces.IBaseObjectwebdav.interfaces.IDAVResourceplone.app.folder.bbb.IArchivableeea.pdf.subtypes.interfaces.ICollectionPDFAwareProducts.CMFCore.interfaces._content.IFolderisheea.workflow.interfaces.IHasMandatoryWorkflowFieldsOFS.interfaces.IFoldereea.progressbar.interfaces.IBaseObjectcollective.quickupload.interfaces.IQuickUploadCapableplone.app.imaging.interfaces.IBaseObjectwebdav.EtagSupport.EtagBaseInterfaceeea.geotags.storage.interfaces.IGeoTaggedOFS.interfaces.IItemplone.uuid.interfaces.IUUIDAwareOFS.interfaces.ITraversableProducts.ATContentTypes.interfaces.folder.IATBTreeFolderOFS.interfaces.IOrderedContainereea.facetednavigation.subtypes.interfaces.IPossibleFacetedNavigablewebdav.interfaces.IDAVCollectioneea.themecentre.interfaces.IThemeTaggableeea.indicators.content.interfaces.IAssessmentAccessControl.interfaces.IRoleManagerAccessControl.interfaces.IPermissionMappingSupporteea.indicators.content.interfaces.IIndicatorAssessmentProducts.Archetypes.interfaces.referenceable.IReferenceableeea.geotags.storage.interfaces.IGeoTaggableProducts.EEAContentTypes.interfaces.IEEAPossibleContentProducts.Archetypes.interfaces.base.IBaseObjecteea.epub.subtypes.interfaces.IEPUBAwareplone.portlets.interfaces.ILocalPortletAssignableeea.pdf.subtypes.interfaces.IPDFAwareplone.app.folder.bbb.IPhotoAlbumAbleOFS.interfaces.IPropertyManagerProducts.Archetypes.interfaces.metadata.IExtensibleMetadataOFS.interfaces.ICopySource100fisheriesmarinenorth seaclimate changeplankton Increases in regional sea temperatures have triggered a major northward movement of warmer-water plankton in the north-east Atlantic and a similar retreat of colder-water plankton to the north. This northerly movement is about 10 o latitude (1 100 km) over the past 40 years, and it seems to have accelerated since 2000. This will have an impact on the distribution of fish in the region. Many species of fish and plankton have shifted their distributions northward. Sub-tropical species are occurring with increasing frequency in European waters and sub-Arctic species are receding northwards. The rate of northward movement of a particular species, the silvery john dory, has been estimated at about 50 km/year. Changes in the geographic distribution of some species of fish have been observed and may affect the management of fisheries. Fisheries regulations in the EU include allocations of quotas based on historic catch patterns, and these may need to be revised. IcelandUnited KingdomBay of BiscayDenmarkGermanyIrelandNetherlandsBelgiumFranceSpainNorth SeaCeltic SeaNorwayPortugalIrish Sea2012-09-11T14:50:58ZNorthward movement of marine species (CLIM 015) - Assessment published Sep 2008alec

Increases in regional sea temperatures have triggered a major northward movement of warmer-water plankton in the north-east Atlantic and a similar retreat of colder-water plankton to the north. This northerly movement is about 10o latitude (1 100 km) over the past 40 years, and it seems to have accelerated since 2000. This will have an impact on the distribution of fish in the region.

Many species of fish and plankton have shifted their distributions northward. Sub-tropical species are occurring with increasing frequency in European waters and sub-Arctic species are receding northwards. The rate of northward movement of a particular species, the silvery john dory, has been estimated at about 50 km/year.

Changes in the geographic distribution of some species of fish have been observed and may affect the management of fisheries. Fisheries regulations in the EU include allocations of quotas based on historic catch patterns, and these may need to be revised.